
mineral
Amethyst (Geode)
Silicon Dioxide (SiO2) with iron impurities
Hardness: 7 on Mohs scale; Color: Purple, violet, to deep lavender; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Purple, violet, to deep lavender
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Purple, violet, to deep lavender; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or cavities (vugs) within igneous rocks, particularly basalt. The purple hue is caused by irradiation of trivalent iron (Fe3+) within the crystal lattice. Most major deposits date back to the Cretaceous period.
Uses & applications
Primary use is in jewelry (faceted or cabochon), ornamental decoration (geodes and cathedrals), and as a popular specimen for mineral collectors.
Geological facts
Until the 18th century, amethyst was included in the cardinal gemstones alongside diamond, ruby, emerald, and sapphire. Large deposits found in Brazil significantly lowered its market value, making it accessible to many collectors.
Field identification & locations
Identify in the field by its distinct purple color, hexagonal prismatic crystal points, and lack of cleavage. Common locations include the Rio Grande do Sul region of Brazil, Artigas in Uruguay, and Ontario, Canada.
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